Titanokorys
| Titanokorys Temporal range:  | |
|---|---|
| The paratype specimen ROMIP 65168; an anterior sclerite | |
| Scientific classification | |
| Domain: | Eukaryota | 
| Kingdom: | Animalia | 
| Phylum: | Arthropoda | 
| Order: | †Radiodonta | 
| Family: | †Hurdiidae | 
| Subfamily: | †Hurdiinae | 
| Genus: | †Titanokorys Caron & Moysiuk, 2021 | 
| Species: | †T. gainesi | 
| Binomial name | |
| †Titanokorys gainesi Caron & Moysiuk, 2021 | |
Titanokorys is a genus of extinct hurdiid (peytoiid) radiodont (a grouping of primitive stem arthropods which lived during the early Paleozoic) that lived during the Miaolingian epoch of the middle Cambrian. It is the largest member of its family from the Cambrian, with an estimated body length of around 50 cm (20 in) long, making it one of the largest animals of the time. It bears a resemblance to the related, and contemporary, genus Cambroraster. Fossils of T. gainesi were first found within the Marble Canyon locality of the Burgess Shale in 2018, however the fossils were not named until 2021 because they were assumed to be giant specimens of Cambroraster.
The taxon is one of several genera of radiodonts known from the Burgess Shale, with some of the others being Cambroraster, Anomalocaris, Peytoia, and Hurdia. Titanokorys is distinguished from other Burgess Shale radiodonts because of its large anterior sclerite (head covering carapace, or H-element) and a pair of spines on the anteroventral sides. Based on the shape of its appendages, Titanokorys is speculated to have used them to sift through the sand looking for prey. It is believed to have fed by using its anterior sclerite to scoop up organisms from the sea floor. Then it would use the endites on its frontal appendages (long grasping structures that all radiodonts possessed) to trap the prey item so it could start consuming it. Because of its size, Titanokorys was one of the dominant predators of the Burgess Shale and one of the largest animals in its ecosystem. However, it is a relatively rare faunal component, suggesting that the Burgess Shale represented the edge of this radiodonts geographic range.